The decay of flexural-gravity waves in long sea-ice transects

Flexural oscillations of floating sea ice sheets induced by ocean waves travelling at the boundary between the ice and the water below can propagate great distances. But, by virtue of scattering, changes of ice thickness and other properties encountered during the journey affect their passage, notwi...

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Bibliographic Details
Published in:Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Vaughan, G., Bennetts, L., Squire, V.
Format: Article in Journal/Newspaper
Language:English
Published: Royal Soc London 2009
Subjects:
Online Access:http://hdl.handle.net/2440/75338
https://doi.org/10.1098/rspa.2009.0187